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Magma batches with distinct petrographic and geochemical characteristics emerged from source zones whose depth progressively increased from 27 to 31 kilometers. The rise of magma of deeper origin is attested by fluid inclusions made of N\n            <jats:sub>2<\/jats:sub>\n            and CO, markers of mantle outgassing. Magma accumulation occurred over different durations at depths of 22 to 27 and 4 to 16 kilometers. Time-integrated magma ascent velocities (including ponding times) were estimated at between 0.01 and 0.1 meters per second. This method is cost-effective and quickly identifies changes in the magma system during an eruption, enhancing petrological monitoring procedures.\n          <\/jats:p>","DOI":"10.1126\/sciadv.adi4300","type":"journal-article","created":{"date-parts":[[2024,2,7]],"date-time":"2024-02-07T19:36:41Z","timestamp":1707334601000},"update-policy":"https:\/\/doi.org\/10.34133\/aaas_crossmark","source":"Crossref","is-referenced-by-count":19,"title":["Toward a near real-time magma ascent monitoring by combined fluid inclusion barometry and ongoing seismicity"],"prefix":"10.1126","volume":"10","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-6990-7610","authenticated-orcid":true,"given":"Vittorio","family":"Zanon","sequence":"first","affiliation":[{"name":"Instituto de Investiga\u00e7\u00e3o em Vulcanologia e Avalia\u00e7\u00e3o de Riscos (IVAR), Universidade dos A\u00e7ores, Rua M\u00e3e de Deus, 9500-123 Ponta Delgada, Portugal."}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-7664-2216","authenticated-orcid":true,"given":"Luca","family":"D\u2019Auria","sequence":"additional","affiliation":[{"name":"Instituto Tecnol\u00f3gico y de Energ\u00edas Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain."},{"name":"Instituto Volcanol\u00f3gico de Canarias (INVOLCAN), 38400 Puerto de la Cruz, Tenerife, Canary Islands, Spain."}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-9801-1581","authenticated-orcid":true,"given":"Federica","family":"Schiavi","sequence":"additional","affiliation":[{"name":"Laboratoire Magmas et Volcans, CNRS, IRD, OPGC, Universit\u00e9 Clermont Auvergne, F-63000 Clermont-Ferrand, France."}]},{"ORCID":"https:\/\/orcid.org\/0009-0003-9649-8228","authenticated-orcid":true,"given":"Klaudia","family":"Cyrzan","sequence":"additional","affiliation":[{"name":"Instituto de Investiga\u00e7\u00e3o em Vulcanologia e Avalia\u00e7\u00e3o de Riscos (IVAR), Universidade dos A\u00e7ores, Rua M\u00e3e de Deus, 9500-123 Ponta Delgada, Portugal."}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6844-9822","authenticated-orcid":true,"given":"Matthew J.","family":"Pankhurst","sequence":"additional","affiliation":[{"name":"Instituto Tecnol\u00f3gico y de Energ\u00edas Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain."},{"name":"Instituto Volcanol\u00f3gico de Canarias (INVOLCAN), 38400 Puerto de la Cruz, Tenerife, Canary Islands, Spain."}]}],"member":"221","reference":[{"key":"e_1_3_2_2_2","doi-asserted-by":"publisher","DOI":"10.1093\/gji\/ggt505"},{"key":"e_1_3_2_3_2","doi-asserted-by":"publisher","DOI":"10.1029\/2018GL080895"},{"key":"e_1_3_2_4_2","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2018.04.025"},{"key":"e_1_3_2_5_2","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2018.01.001"},{"key":"e_1_3_2_6_2","doi-asserted-by":"publisher","DOI":"10.1126\/sciadv.adg4813"},{"key":"e_1_3_2_7_2","doi-asserted-by":"publisher","DOI":"10.1016\/j.jvolgeores.2004.08.002"},{"key":"e_1_3_2_8_2","doi-asserted-by":"publisher","DOI":"10.1007\/s00410-018-1487-9"},{"key":"e_1_3_2_9_2","doi-asserted-by":"publisher","DOI":"10.1016\/j.jvolgeores.2008.11.010"},{"key":"e_1_3_2_10_2","doi-asserted-by":"publisher","DOI":"10.1029\/2005JB003934"},{"key":"e_1_3_2_11_2","doi-asserted-by":"publisher","DOI":"10.1126\/science.aaz0147"},{"key":"e_1_3_2_12_2","doi-asserted-by":"publisher","DOI":"10.1038\/s41586-022-04981-x"},{"key":"e_1_3_2_13_2","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2022.117793"},{"key":"e_1_3_2_14_2","doi-asserted-by":"crossref","unstructured":"K. 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